Upload
juro
View
26
Download
0
Tags:
Embed Size (px)
DESCRIPTION
The Rock Cycle. Chapters 5 & 6. What are the types of rock?. Igneous rocks Form from cooling magma Recall: magma is molten material beneath Earth’s surface Sedimentary rocks Form from cementing and compacting pieces of sediment - PowerPoint PPT Presentation
Citation preview
TheRock CycleChapters 5 & 6
What are the types of rock?
• Igneous rocks• Form from cooling magma• Recall: magma is molten material
beneath Earth’s surface• Sedimentary rocks
• Form from cementing and compacting pieces of sediment
• Sediment is pieces of solid material deposited on Earth’s surface
• Metamorphic rocks• Rocks that have been changed
from heat and pressure
Igneous Rocks
• Formation of igneous rock• Intrusive
• Formed by magma that cools slowly
• Formed beneath the Earth’s surface
• Coarse-grained• Ex. granite
• Extrusive• Formed by magma that cools
quickly• Formed above the Earth’s
surface• Fine-grained• Ex. Rhyolite
• Properties of igneous rock• Mineral composition
• Light colored = felsic• Dark colored = mafic
• Grain size• Coarse-grained = intrusive• Fine-grained = extrusive
Sedimentary Rocks
• Formation of sedimentary rock• Weathering produces sediments
• Physical weathering• Happens when rock
fragments break off.• Ex.
• Temperature changes expand or contract rock
• Living organisms like trees crack rocks
• Chemical weathering• Happens when the minerals
in rocks are chemically changed
• Ex.• Dissolving• Oxidation (rust)
• Erosion transports weathered sediments from one place to another
• Types of erosion• Wind• Moving water• Gravity• Glaciers
• Deposition is when sediments are laid down on the ground or under water
• This can cause sorting of sediments into layers, which is called bedding.
• Deposited sediments become buried
http://www.classzone.com/books/earth_science/terc/content/visualizations/es0604/es0604page01.cfm?chapter_no=visualization
• Lithification happens when the weight of overlaying sediments forces grains closer together.
• Water is pressed out• Sand is compacted• High temperatures (~3-4km
deep) cause cementation• New minerals can grow
between cemented sediments
• Properties of sedimentary rock
• Clastic—formed from deposits of loose sediments
http://www.classzone.com/books/earth_science/terc/content/visualizations/es0605/es0605page01.cfm?chapter_no=visualization• Chemical—formed from
precipitation of minerals dissolved in water
• Organic—formed from accumulation and lithification of dead organisms
• Ex. coal
Metamorphic Rocks
• Formation of metamorphic rocks
• High temperatures and pressures increase with depth
• High temperature comes from Earth’s internal heat or intruding magma.
• High pressure comes from overlying rock or the compression of mountain building
• Rocks do not melt, but change in texture, mineralogy, or chemical composition
http://www.classzone.com/books/earth_science/terc/content/visualizations/es0607/es0607page01.cfm?chapter_no=visualization
• Properties of metamorphic rocks
• Texture• Foliated—wavy layers and
bands of minerals• Nonfoliated—minerals form
blocky crystals• Mineral composition
• Heat & pressure can change one mineral into another
• Chemical composition• Hot fluids go in and out of
the rock during metamorphism, changing its chemistry
What is the rock cycle?
• The rock cycle is the continuous changing and remaking of rocks
• Any type of rock can turn into any other type of rock
• Matter making up rocks is neither crated nor destroyed, but simply changed.
• Processes that power the rock cycle
• Internal processes• Uplift• Heat & pressure• Melting• Cooling & crystallization
• External processes• Uplift• Weathering & erosion• Deposition, burial, & lithification